Noun:

ಬೆಚ್ಚಗಿನ ಮುಂಭಾಗ,

warm front's Usage Examples:

Cold fronts often follow a warm front or squall line.

warm front is cooler than the cool air ahead of the warm front and plows under both air masses.

Extratropical cyclones are fed by inflow focused along their cold front and warm fronts.

They can indicate an approaching warm front; however, they can also be an indication that fair weather will follow.

In areas where cold fronts catch up to the warm front, the occluded front develops.

Clouds ahead of the warm front are mostly stratiform, and rainfall gradually increases as the front approaches.

occlusions move faster than warm fronts and warm occlusions, because the dense air behind them can lift as well as push the warmer air.

be preceded by squall lines, while warm fronts are usually preceded by stratiform precipitation and fog.

precipitation bands in an otherwise stable region, such as in front of a warm front.

The classical view of an occluded front is that they are formed when a cold front overtakes a warm front, such that the warm air is separated (occluded).

classical view of an occluded front is that they are formed when a cold front overtakes a warm front, such that the warm air is separated (occluded) from the.

They are also often seen underneath the cirrostratus and altostratus sheets that often precede a warm front, as these higher clouds decrease.

A warm front is a density discontinuity located at the leading edge of a homogeneous warm air mass, and is typically located on the equator-facing edge.

Synonyms:

forefront, forepart, head, side, face, front end,

Antonyms:

rear, starboard, reverse, larboard, bottom,